Technical note: Sea salt interference with black carbon quantification in snow samples using the single particle soot photometer
After aerosol deposition from the atmosphere, black carbon (BC) takes part in the snow albedo feedback contributing to the modification of the Arctic radiative budget. With the initial goal of quantifying the concentration of BC in the Arctic snow and subsequent climatic impacts, snow samples were c...
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ftcopernicus:oai:publications.copernicus.org:acp93251 2023-05-15T13:11:44+02:00 Technical note: Sea salt interference with black carbon quantification in snow samples using the single particle soot photometer Zanatta, Marco Herber, Andreas Jurányi, Zsófia Eppers, Oliver Schneider, Johannes Schwarz, Joshua P. 2021-06-17 application/pdf https://doi.org/10.5194/acp-21-9329-2021 https://acp.copernicus.org/articles/21/9329/2021/ eng eng doi:10.5194/acp-21-9329-2021 https://acp.copernicus.org/articles/21/9329/2021/ eISSN: 1680-7324 Text 2021 ftcopernicus https://doi.org/10.5194/acp-21-9329-2021 2021-06-21T16:22:14Z After aerosol deposition from the atmosphere, black carbon (BC) takes part in the snow albedo feedback contributing to the modification of the Arctic radiative budget. With the initial goal of quantifying the concentration of BC in the Arctic snow and subsequent climatic impacts, snow samples were collected during the research vessel (R/V) Polarstern expedition of PASCAL (Physical Feedbacks of Arctic Boundary Layer, Sea Ice, Cloud and Aerosol; Polarstern cruise 106) in the sea-ice-covered Fram Strait in early summer 2017. The refractory BC (rBC) content was then measured in the laboratory of the Alfred Wegener Institute with the single particle soot photometer (SP2). Based on the strong observational correlations between both rBC concentration and rBC diameter with snow salinity, we hypothesize a salt-induced matrix effect interfering with the SP2 analysis. This paper evaluates the impact of sea salt, based on the measurement of electrical conductivity ( κ ) in water samples, on rBC measurements made with a SP2 nebulizer technique. Under realistic salinity conditions, laboratory experiments indicated a dramatic six-fold reduction in observed rBC concentration with increasing salinity. In the salinity conditions tested in the present work (salt concentration below 0.4 g L −1 ) the impact of salt on the nebulization of water droplets might be negligible. However, the SP2 mass detection efficiency systematically decreased with increasing salinity, with the smaller rBC particles being preferentially undetected. The high concentration of suspended salt particles and the formation of thick salt coatings on rBC cores caused problems in the SP2 analog-to-digital conversion of the signal and incandescence quenching, respectively. Changes to the signal acquisition parameters and the laser power of the SP2 improved the mass detection efficiency, which, nonetheless, stayed below unity. The present work provides evidence that a high concentration of sea salt undermines the quantification of rBC in snow performed with the SP2 nebulizer system described here. This interference has not been previously reported and might affect the future such analysis of rBC particles in snow collected, especially over sea ice or coastal regions strongly affected by sea salt deposition. Text albedo Arctic black carbon Fram Strait Sea ice Copernicus Publications: E-Journals Arctic Atmospheric Chemistry and Physics 21 12 9329 9342 |
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Open Polar |
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Copernicus Publications: E-Journals |
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ftcopernicus |
language |
English |
description |
After aerosol deposition from the atmosphere, black carbon (BC) takes part in the snow albedo feedback contributing to the modification of the Arctic radiative budget. With the initial goal of quantifying the concentration of BC in the Arctic snow and subsequent climatic impacts, snow samples were collected during the research vessel (R/V) Polarstern expedition of PASCAL (Physical Feedbacks of Arctic Boundary Layer, Sea Ice, Cloud and Aerosol; Polarstern cruise 106) in the sea-ice-covered Fram Strait in early summer 2017. The refractory BC (rBC) content was then measured in the laboratory of the Alfred Wegener Institute with the single particle soot photometer (SP2). Based on the strong observational correlations between both rBC concentration and rBC diameter with snow salinity, we hypothesize a salt-induced matrix effect interfering with the SP2 analysis. This paper evaluates the impact of sea salt, based on the measurement of electrical conductivity ( κ ) in water samples, on rBC measurements made with a SP2 nebulizer technique. Under realistic salinity conditions, laboratory experiments indicated a dramatic six-fold reduction in observed rBC concentration with increasing salinity. In the salinity conditions tested in the present work (salt concentration below 0.4 g L −1 ) the impact of salt on the nebulization of water droplets might be negligible. However, the SP2 mass detection efficiency systematically decreased with increasing salinity, with the smaller rBC particles being preferentially undetected. The high concentration of suspended salt particles and the formation of thick salt coatings on rBC cores caused problems in the SP2 analog-to-digital conversion of the signal and incandescence quenching, respectively. Changes to the signal acquisition parameters and the laser power of the SP2 improved the mass detection efficiency, which, nonetheless, stayed below unity. The present work provides evidence that a high concentration of sea salt undermines the quantification of rBC in snow performed with the SP2 nebulizer system described here. This interference has not been previously reported and might affect the future such analysis of rBC particles in snow collected, especially over sea ice or coastal regions strongly affected by sea salt deposition. |
format |
Text |
author |
Zanatta, Marco Herber, Andreas Jurányi, Zsófia Eppers, Oliver Schneider, Johannes Schwarz, Joshua P. |
spellingShingle |
Zanatta, Marco Herber, Andreas Jurányi, Zsófia Eppers, Oliver Schneider, Johannes Schwarz, Joshua P. Technical note: Sea salt interference with black carbon quantification in snow samples using the single particle soot photometer |
author_facet |
Zanatta, Marco Herber, Andreas Jurányi, Zsófia Eppers, Oliver Schneider, Johannes Schwarz, Joshua P. |
author_sort |
Zanatta, Marco |
title |
Technical note: Sea salt interference with black carbon quantification in snow samples using the single particle soot photometer |
title_short |
Technical note: Sea salt interference with black carbon quantification in snow samples using the single particle soot photometer |
title_full |
Technical note: Sea salt interference with black carbon quantification in snow samples using the single particle soot photometer |
title_fullStr |
Technical note: Sea salt interference with black carbon quantification in snow samples using the single particle soot photometer |
title_full_unstemmed |
Technical note: Sea salt interference with black carbon quantification in snow samples using the single particle soot photometer |
title_sort |
technical note: sea salt interference with black carbon quantification in snow samples using the single particle soot photometer |
publishDate |
2021 |
url |
https://doi.org/10.5194/acp-21-9329-2021 https://acp.copernicus.org/articles/21/9329/2021/ |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
albedo Arctic black carbon Fram Strait Sea ice |
genre_facet |
albedo Arctic black carbon Fram Strait Sea ice |
op_source |
eISSN: 1680-7324 |
op_relation |
doi:10.5194/acp-21-9329-2021 https://acp.copernicus.org/articles/21/9329/2021/ |
op_doi |
https://doi.org/10.5194/acp-21-9329-2021 |
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Atmospheric Chemistry and Physics |
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21 |
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12 |
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9329 |
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9342 |
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1766248763651784704 |